首页 | 本学科首页   官方微博 | 高级检索  
   检索      

不同海拔对福建戴云山黄山松林土壤微生物生物量和土壤酶活性的影响
引用本文:赵盼盼,周嘉聪,林开淼,林伟盛,袁萍,曾晓敏,苏莹,徐建国,陈岳民,杨玉盛.不同海拔对福建戴云山黄山松林土壤微生物生物量和土壤酶活性的影响[J].生态学报,2019,39(8):2676-2686.
作者姓名:赵盼盼  周嘉聪  林开淼  林伟盛  袁萍  曾晓敏  苏莹  徐建国  陈岳民  杨玉盛
作者单位:福建师范大学湿润亚热带生态地理过程教育部重点实验室;福建师范大学地理研究所;福建戴云山国家级自然保护区管理局
基金项目:国家自然科学基金项目(31670620);海峡联合基金项目(U1505233)
摘    要:温度、水分等多种环境因子随海拔梯度发生变化,会直接或间接影响土壤微生物生物量、群落结构以及土壤酶活性。然而关于中亚热带地区山地森林生态系统土壤酶活性变化响应的研究还是相对匮乏。戴云山山脉是中国最大的黄山松种质基因基地,本研究以中亚热带戴云山1300 m (L)、1450 m(M)、1600 m(H)的黄山松(Pinus taiwanensis)为研究对象,探究不同海拔下土壤微生物生物量和土壤酶活性如何变化及驱动土壤酶活性变化的主要的环境因子。结果表明:海拔梯度对淀积层(B)土壤的酶活性影响整体较小,在淋溶层(A)土壤中,随海拔升高,纤维素水解酶(β-葡糖苷酶(βG)、纤维素水解酶(CBH))显著降低,因此使土壤可溶性碳(DOC)和微生物生物量碳(MBC)随海拔升高有下降趋势。尽管酸性磷酸酶活性(ACP)随海拔升高显著增加,然而有效磷(AP)无显著变化。此外随海拔升高,微生物生物量氮(MBN)、微生物生物量磷(MBP)显著降低。冗余分析(RDA)结果发现,MBP和碳/氮比(C/N)是影响A层中土壤酶活性变化最重要的因子,而在B层中,土壤含水量(WC)和MBP对土壤酶活性起主要作用。研究表明,磷限制的亚热带地区,无机磷很容易被铁铝固定,MBP可以对土壤中的有效磷进行补充,成为影响本地区酶活性的主要因素。随海拔海拔降低,土壤有机碳、氮分解相关酶活性较高,从而加速了土壤碳、氮周转。因此,探究不同海拔梯度酶活性变化为预测中亚热带亚山地森林生态系统土壤碳、氮、磷养分循环提供了重要的理论依据,也为戴云山自然保护区黄山松林管理提供一定的科学依据。

关 键 词:海拔  酶活性  微生物生物量
收稿时间:2018/5/11 0:00:00
修稿时间:2018/11/5 0:00:00

Effects of different altitudes on soil microbial biomass and enzyme activities in Pinus taiwanensis forests on Daiyun Mountain, Fujian Province
ZHAO Panpan,ZHOU Jiacong,LIN Kaimiao,LIN Weisheng,YUAN Ping,ZENG Xiaomin,SU Ying,XU Jianguo,CHEN Yuemin and YANG Yusheng.Effects of different altitudes on soil microbial biomass and enzyme activities in Pinus taiwanensis forests on Daiyun Mountain, Fujian Province[J].Acta Ecologica Sinica,2019,39(8):2676-2686.
Authors:ZHAO Panpan  ZHOU Jiacong  LIN Kaimiao  LIN Weisheng  YUAN Ping  ZENG Xiaomin  SU Ying  XU Jianguo  CHEN Yuemin and YANG Yusheng
Institution:Key Laboratory for Humid Subtropical Eco-geographical Processes of the Ministry of Education, Fujian Normal University, Fuzhou 350007, China;Institute of Geography, Fujian Normal University, Fuzhou 350007, China,Key Laboratory for Humid Subtropical Eco-geographical Processes of the Ministry of Education, Fujian Normal University, Fuzhou 350007, China;Institute of Geography, Fujian Normal University, Fuzhou 350007, China,Key Laboratory for Humid Subtropical Eco-geographical Processes of the Ministry of Education, Fujian Normal University, Fuzhou 350007, China;Daiyun Mountain National Nature Reserve Administration Bureau, Quanzhou 362500, China,Key Laboratory for Humid Subtropical Eco-geographical Processes of the Ministry of Education, Fujian Normal University, Fuzhou 350007, China;Institute of Geography, Fujian Normal University, Fuzhou 350007, China,Key Laboratory for Humid Subtropical Eco-geographical Processes of the Ministry of Education, Fujian Normal University, Fuzhou 350007, China;Institute of Geography, Fujian Normal University, Fuzhou 350007, China,Key Laboratory for Humid Subtropical Eco-geographical Processes of the Ministry of Education, Fujian Normal University, Fuzhou 350007, China;Institute of Geography, Fujian Normal University, Fuzhou 350007, China,Key Laboratory for Humid Subtropical Eco-geographical Processes of the Ministry of Education, Fujian Normal University, Fuzhou 350007, China;Institute of Geography, Fujian Normal University, Fuzhou 350007, China,Daiyun Mountain National Nature Reserve Administration Bureau, Quanzhou 362500, China,Key Laboratory for Humid Subtropical Eco-geographical Processes of the Ministry of Education, Fujian Normal University, Fuzhou 350007, China;Institute of Geography, Fujian Normal University, Fuzhou 350007, China and Key Laboratory for Humid Subtropical Eco-geographical Processes of the Ministry of Education, Fujian Normal University, Fuzhou 350007, China;Institute of Geography, Fujian Normal University, Fuzhou 350007, China
Abstract:
Keywords:altitudes  soil enzyme activities  soil microbial biomass
本文献已被 CNKI 等数据库收录!
点击此处可从《生态学报》浏览原始摘要信息
点击此处可从《生态学报》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号